Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering.

Slides:



Advertisements
Similar presentations
Weathering Processes.
Advertisements

Sedimentary rocks Geology 101.
Weathering Soils Mass Movement Chapter 8. TOPIC 1 Weathering- The break-up of rock due to exposure to the atmosphere. Depth of rock a factor. –GRANITE.
Weathering of Rocks. Exam 1 Why we see weathering 1.Most minerals are not stable at the Earth’s surface 2.The Earth wants to be flat – lowest energy.
Weathering. Sedimentary Cover + Sedimentary rocks form a veneer over much older igneous and metamorphic “basement” rocks. + This veneer varies in thickness.
WEATHERING: - cementation and compaction of weathered material on the earth’s surface creates sedimentary rocks Weathering is the process of breaking.
Chemical & Mechanical Weathering How is soil formed?
Weathering and Soils. Marble headstones in Southern Vermont Weathering and Soils Granite headstone in Southern Vermont.
Rocks and Weathering Chapter 8.1.
Chemical Weathering and Soils Chapter 3. Weathering Igneous minerals formed out of equilibrium with Earth’s surface WEATHERING converts less-stable minerals.
Ch 9. Weathering A. Mechanical Weathering B. Chemical Weathering C. Soil.
Weathering & Soils Mr. Manzo.
Weathering and Erosion
Weathering
Where are we??? Earth’s matter & structure Rock forming processes
Chapter 6 Weathering and Soil
Weathering and Erosion
Ch 5 – Weathering & Erosion
Weathering and Soils The Rotting Earth Physical weathering processes Chemical weathering processes Factors affecting weathering Soil: The residue of weathering.
Chapter Five Weathering: The Breakdown of Rocks. CHAPTER 5: WEATHERING: THE BREAKDOWN OF ROCKS A) WEATHERING: PROCESS BY WHICH ROCKS AND MINERALS BREAK.
The Art of Breaking things… Weathering and Soil. Weathering ► Weathering is the physical breakdown (disintegration) and chemical alteration (decomposition)
Chemical Weathering. Weathering What is weathering? –Weathering is the disintegration and decomposition of rock at or near the surface of the earth.
Formation of Sedimentary Rocks
Weathering and Soil. Types of Weathering Chemical Weathering: a rock being changed into 1 or more new compounds Oxidation- turns the rock into a rusty.
Chapter 16: Weathering and Erosion Copyright © 2007 by W. H. Freeman & Company With adaptaions from lectures by Peter Copeland Bill Dupré.
Chapter 7- Weathering, Erosion and Soil
Classroom presentations to accompany Understanding Earth, 3rd edition prepared by Peter Copeland and William Dupré University of Houston Chapter 6 Weathering.
Weathering, Erosion, Soil and Sedimentary Rocks Chapter 8 & 5.
Earth’s Surface is Constantly Changing
WEATHERING GEOLOGY NOTES Chapter 5 WEATHERING 4 Breakdown of rock due to weather 4 no visible motion.
What is Weathering? Weathering is the chemical or physical breakdown of a rock or mineral due to exposure to the atmosphere.
Weathering,Soil and Glacial Movement Ch. 14,15. What Physical Properties Affect Rocks Near the Surface? There are many processes that break rocks apart.
Weathering and Soils GEOLOGY TODAY - Chapter 7 Barbara W. Murck Brian J. Skinner N. Lindsley-Griffin, 1999 Acid Rain Damage Soil Profile.
Chapter 5 Weathering and Soil GEOL 101 Introductory Geology.
Soil Origin and Development
Chapter 5 Weathering and Soil
Weathering Weathering is the physical breakdown and chemical alteration of rocks and minerals. Weathering happens on or near the surface. Weathering is.
Ch 14 Weathering Two Types: 1.Physical or Mechanical 2.Chemical.
Weathering of Rocks. Why we see weathering 1.Most minerals are not stable at the Earth’s surface 2.The Earth wants to be flat – lowest energy state Topography.
The speed rocks weather depends on a few factors… check em out.
Weathering and Soil Geology 101 Ted Brewster.
THE ROCK CYCLE. Sediment is produced either directly or indirectly by the weathering and erosion of pre-existing rocks. Grains can originate as: A)Broken.
© 2011 Pearson Education, Inc. Weathering and Soil Earth, 10e - Chapter 6.
Earth Science Unit 1.4: Weathering and Soils. The Rock Cycle.
CH 12 Weathering, Soil, Mass Movements (Gravity) Earth’s surface is constantly changing. Earth’s surface is constantly changing. Weathering = breaking.
Weathering Review Vocabulary acid: solution that contains hydrogen ions Weathering breaks down materials on or near Earth’s surface.
Weathering & Soils Mr. Manzo. Erosion Features of Bryce Canyon Nat. Park in Utah.
Frost Heaving. Plant Roots (Root Pry) Talus Water.
Chapter 4 – Weathering Sedimentary rocks are composed of sediment. Sediment forms at or near earth’s surface through the processes of weathering, transportation,
Weathering, Soil, and Mass Movements Chapter 5. Mechanical Weathering physical forces break rock into smaller and smaller pieces.
SOIL ORIGIN AND NATURE, FORMATION OF SOILS. Soil develops from parent material by the processes of soil formation The process of formation soil from the.
Weathering and Soil. Earth’s External Processes  weathering—the physical breakdown and chemical decomposition of rock  mass wasting—the transfer of.
Rocks and Weathering Chapter 8.1.
Weathering, Erosion, and Soil
Weathering.
What’s it good for, anyway?
Weathering of Rocks.
Chapter 12: Weathering & Erosion
Weathering.
Ch 5 Weathering, soils, and erosion
Weathering and Soil Chapter 7.
Ch 5 – Weathering & Erosion
Weathering Weathering - processes at or near Earth’s surface that cause rocks and minerals to break down Erosion - process of removing Earth materials.
Sedimentary rocks Geology 115.
Soil Brainpop Weathering Brainpop
Ch 12: Weathering and Erosion.
Weathering and Erosion
Ch 5 – Weathering & Erosion
THE EARTH WILL NOT BE HAPPY UNTIL IT IS FLAT
Chapter Five Weathering: The Breakdown of Rocks
Presentation transcript:

Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering Products - Soils - Paleosols Text: Manual p. 15, 89; Boggs Ch.1,

Causes of Color yellowgoethite, jarositecement brownFe-oxidescement redFe-oxidescement, coatings purplehematite (coarse)cement pinkK-feldspar, hematitecement, framework whitekaolinite, gypsum, no organics cement, bleaching greenglauconite, chlorite, illitecement, framework blackorganics, oil, heavy minerals, pyrite, Mn-oxide cement, framework colormineraloccurrence

Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering Products - Soils - Paleosols Text: Manual p. 15, 89; Boggs Ch.1,

Trace Fossils Ichnofacies (Boggs, p. 118) Environment

Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering Products - Soils - Paleosols Text: Manual p. 15, 89; Boggs Ch.1,

Physical Weathering no change in mineral / chemical composition Physical Weathering: Break-down rock into smaller pieces

Physical Weathering 1. Granite 2. Partially-Weathered Granite 3. Granite Grus

roots / lichens freeze-thaw wet-dry hot-cold Physical Weathering

Exfoliation Enchanted Rock batholith

Physical Weathering Spheroidal Weathering Costa Rica

Physical Weathering Painted Desert, Utah Gullying

Bryce Canyon Physical Weathering

Chemical Weathering alter chemical and mineral composition disrupt fabrics Chemical Weathering: Dissolution and/or crystallization of new minerals

Chemical Weathering Feldspar + H + + H 2 O  kaolinite + silicic acid + K + or Na 2+ Hydrolysis: H + breaks down silicates

Chemical Weathering pyrite Oxidation / Reduction: O alters Fe silicates and S minerals pyrite pyrite  hematite silicate mineral  Fe-oxide

Chemical Weathering Fe-oxide Stains (E. McBride) Bastrop, TX

Chemical Weathering Solution: dissolve in water pyrite (E McBride) Limestone Karen Rills calcite / dolomite gypsum halite

Physical/Chemical Weathering bench slope cliff Differential Weathering Grand Canyon

Physical/Chemical Weathering Differential Weathering “Toadstools” Utah

Physical/Chemical Weathering Differential Weathering burrows

Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering Products - Soils - Paleosols Text: Manual p. 15, 89; Boggs Ch.1,

clastic sediments residues (source rock) secondary minerals ions in solution Weathering Products Soils and Sed. Rocks

Weathering Products Terrigenous Clastic Sediments

Weathering Products Evaporites Death Valley, CA Chemical Sediments courtesy Matt Campbell Cements (M. Campbell)

Soils mineral residues rock fragments organics Horizons Soil Profile

Soils Horizons Soil Profile O - organic matter A - topmost mineral horizon E - (eluvial) leaching B - (illuvial) accumulation C - weathered bedrock R - bedrock

Soils bedrock time climate topography

Pedocal Soils Pedalfer Soils 30 inches of rain per year Soils

color texture structure consistency contacts

Soils Texture

FIGURE 3-26FIGURE 3-26 FIGURE 3-28FIGURE 3-28 FIGURE 3-30FIGURE 3-30 FIGURE 3-29FIGURE 3-29 columnar crumb platy blocky Soils Structure

ClassesDescription Non-plastic A roll 4 cm long and 6 mm thick that supports its own weight held on end cannot be formed. Slightly plastic A roll 4 cm long and 6 mm thick can be formed and, if held on end, will support its own weight. A roll 4 mm thick will not support its own weight. Moderately plastic A roll 4 cm long and 4 mm thick can be formed and will support its own weight, but a roll 2 mm thick will not support its own weight. Very plastic A roll 4 cm long and 2 mm thick can be formed and will support its own weight. Consistency: Plasticity Soils

Standard USDA Soil Description Form Soils

Color, Trace Fossils, Weathering, and Soils Causes of Color Common Trace Fossils Weathering Processes - Physical Weathering - Chemical Weathering Weathering Products - Soils - Paleosols Text: Manual p. 15, 89; Boggs Ch.1,

Paleosols

colors (red, green, purple) root casts caliche vertical streaks mottled bedding

Paleosols Paleosols Painted Desert, AZ

Root Casts Paleosol, near Hunt, TX Paleosols

vertical streaks (bleaching) (E. McBride) Paleosol Bastrop, TX

Paleosols (E. McBride) “terra rossa” fill

Reference Soil Survey Manual, 1993, Soil Conservation Service, USDA Handbook 18.